Seismic imaging: From classical to adjoint tomography
Q Liu, YJ Gu - Tectonophysics, 2012 - Elsevier
Seismic tomography has been a vital tool in probing the Earth's internal structure and
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …
Integrating electromagnetic data with other geophysical observations for enhanced imaging of the earth: a tutorial and review
M Moorkamp - Surveys in Geophysics, 2017 - Springer
In this review, I discuss the basic principles of joint inversion and constrained inversion
approaches and show a few instructive examples of applications of these approaches in the …
approaches and show a few instructive examples of applications of these approaches in the …
Transdimensional inversion of receiver functions and surface wave dispersion
T Bodin, M Sambridge, H Tkalčić… - … research: solid earth, 2012 - Wiley Online Library
We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …
A framework for 3-D joint inversion of MT, gravity and seismic refraction data
M Moorkamp, B Heincke, M Jegen… - Geophysical Journal …, 2011 - academic.oup.com
We present a 3-D joint inversion framework for seismic, magnetotelluric (MT) and scalar and
tensorial gravity data. Using large-scale optimization methods, parallel forward solvers and …
tensorial gravity data. Using large-scale optimization methods, parallel forward solvers and …
The seismic mid-lithosphere discontinuity
Seismic S-wave receiver functions (SRF) are a uniquely powerful tool for imaging velocity
discontinuities within the upper mantle. SRF data frequently contain negative phases at …
discontinuities within the upper mantle. SRF data frequently contain negative phases at …
Joint inversion of surface wave dispersion and receiver functions: a Bayesian Monte-Carlo approach
W Shen, MH Ritzwoller… - Geophysical Journal …, 2013 - academic.oup.com
A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …
Surface wave tomography: imaging of the lithosphere–asthenosphere boundary beneath central and southern Africa?
S Fishwick - Lithos, 2010 - Elsevier
The lithosphere–asthenosphere boundary (LAB) remains a controversial subject in Earth
sciences, and beneath cratonic regions appears to be a particularly difficult boundary to …
sciences, and beneath cratonic regions appears to be a particularly difficult boundary to …
Model fusion and joint inversion
E Haber, M Holtzman Gazit - Surveys in Geophysics, 2013 - Springer
Inverse problems are inherently non-unique, and regularization is needed to obtain stable
and reasonable solutions. The regularization adds information to the problem and …
and reasonable solutions. The regularization adds information to the problem and …
[PDF][PDF] 深部探测揭示中国地壳结构, 深部过程与成矿作用背景
董树文, 李廷栋, 陈宣华, 高锐, 吕庆田, 石耀霖… - 地学前缘, 2014 - researchgate.net
深部探测技术与实验研究专项(SinoProbe; 以下简称“专项”) 是目前中国实施的规模最大的地球
科学研究计划之一, 涉及从地表到深部的地质, 地球物理和地球化学多学科多领域探测实验 …
科学研究计划之一, 涉及从地表到深部的地质, 地球物理和地球化学多学科多领域探测实验 …
The role of electrical anisotropy in magnetotelluric responses: from modelling and dimensionality analysis to inversion and interpretation
A Martí - Surveys in Geophysics, 2014 - Springer
The study of electrical anisotropy in the Earth, defined as the electrical conductivity varying
with orientation, has experienced important advances in the last years regarding the …
with orientation, has experienced important advances in the last years regarding the …